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unit 3 vocab rodney
plate tectonics
Term | Definition |
---|---|
Asthenosphere | the upper layer of the earth's mantle, below the lithosphere, in which there is relatively low resistance to plastic flow and convection is thought to occur. |
Subduction | the sideways and downward movement of the edge of a plate of the earth's crust into the mantle beneath another plate. |
Mantle convection | Mantle convection is the very slow creeping motion of Earth's solid silicate mantle caused by convection currents carrying heat from the interior to the planet's surface. |
Ridge push | Ridge push (also known as gravitational sliding) or sliding plate force is a proposed driving force for plate motion in plate tectonics that occurs at mid-ocean ridges |
Slab pull | What is Slab Pull? Slab pull is the pulling force exerted by a cold, dense oceanic plate plunging into the mantle due to its own weight. |
Tectonic plate | Plate tectonics is a scientific theory describing the large-scale motion of seven large plates and the movements of a larger number |
Convergent boundary | A convergent boundary is an area on Earth where two or more lithospheric plates collide. One plate eventually slides beneath the other causing a process known as subduction. |
Divergent boundary | In plate tectonics, a divergent boundary or divergent plate boundary (also known as a constructive boundary or an extensional boundary) is a linear feature that exists |
Transform boundary | Transform boundaries are places where plates slide sideways past each other. At transform boundaries lithosphere is neither created nor destroyed. |
earthquake | a sudden and violent shaking of the ground, sometimes causing great destruction, as a result of movements within the earth's crust or volcanic action. |
volcano | A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape |